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Identification of the geochemical processes in coastal groundwater using hydrogeochemical and isotopic data: A Case study of the Gadilam river basin in southern India

机译:利用水文地球化学和同位素数据识别沿海地下水的地球化学过程:以印度南部加迪兰姆河流域为例

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摘要

The Gadilam river basin in Tamilnadu is characterized by different geological formation viz. Archaean, Cretaceous, Tertiary to Recent Alluvium and groundwater serves as the major source for domestic, agriculture and other water-related activities. Forty four groundwater samples were collected during summer and post monsoon. Twenty three samples were analysed for stable isotopes (δ~(18)O and δD). Geochemical signatures of groundwater were used to identify the chemical processes that control hydrogeochemsitry. Chemical parameters of groundwater such as pH, EC, TDS, Na~+, K~+, Ca~+, Mg~+, HCO_3~-, SO_4 , PO_4~- and H_4SiO_4 were determined. Interpretation of hydrogeochemical data ascribes that secondary leaching, saline water intrusion and anthropogenic impact in this regime. Interpretation of δ~(18)O and δD indicates recharge from the meteoric water in Tertiary aquifer and from evaporated water in Alluvium aquifer.
机译:泰米尔纳德邦的加迪兰姆河流域具有不同的地质构造特征。古生界,白垩纪,第三纪至最近的冲积层和地下水是家庭,农业和其他与水有关的活动的主要来源。在夏季和季风之后收集了44个地下水样品。分析了23个样品的稳定同位素(δ〜(18)O和δD)。地下水的地球化学特征被用来识别控制水文地球化学的化学过程。确定了地下水的化学参数,如pH,EC,TDS,Na〜+,K〜+,Ca〜+,Mg〜+,HCO_3〜-,SO_4,PO_4〜-和H_4SiO_4。对水文地球化学数据的解释认为,在这种情况下,二次浸出,盐水入侵和人为影响。解释δ〜(18)O和δD表示从第三纪含水层中的陨石水和冲积层中的蒸发水补给。

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